                         ˿µϣ20061231գ

06.12.31, 桶һһϯ̸ۺ󣺶ԱȲܱ١ʶƶ
06.12.31, սѡӡĽѽںҽˮĶλ
06.12.31, ˮαѧڷ
06.12.31, ġҾȻһ־磡
06.12.31, blueseaαѧ¼ӦеĿѧѧ߷˼һ¡
06.12.31, пƼѧѧ³Ϯ̨ѧߵ
06.12.31, ѧһͶ
06.12.31, jianߡ𣿡
06.12.31, 컢ЦХΪд̤߼
06.12.31, һxysߡҩ˵䡷
06.12.31, Źҫҵܺá
06.12.31, Ľɡġɫ֤Ĵ
06.12.31, Yushӹɫ֤ɫĻ
06.12.31, ƽ®ǿҽָ崫ͳ
06.12.31, x8b8x8˼ҹΡ
06.12.31, С״桰Ҽߡͥҽѧרҵ÷ٺͼֱѶ

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

һһϯ̸ۺ󣺶ԱȲܱ١ʶƶ

ߣ

30շӲαѧǷкͳĻƼµĵһϰ
ααԪԬȻ羴֮⣬к
ͷԣֵǿѧʵǡˡֱҪĴݡǫ顢Ϭׯ
ءԱ֮£СƽȻαȻ˻߿̸СһĿ

ЦСƽ˵ûжϿѧĶԴ˵ʽ߼
߼ԭʼ߼קһʲô˵֣ѵԬ˵߼û
㲻˳Ծĵز

ڿ˵ܰѡǿѧαѧ򣬼ֱĪ˼ά
ҵ㣺ȻǿѧˣͲǿѧȴӲ˵Լǡѧ
ǡαѧʲôҲáԭʼ߼Ľͷ
ǵغЩʣΪüƣֲֳ˵ķ
ԣǻ鸡ʵ󾭹ϸĿѧѵѧ߷ȡ
ĻӣȻΪڡǶԬ裬
Ҳɼйƭӵг̶ȡ

αһλոı֣һ仰Ȼ˵ǣеĿѧ¶
еĿѧҵģԾѾҵĸˡ

ѵıҲǳʡ˵Լǡ500һ10֤
°ͺղ롱ڹѧһԪһʮλ
ԲԱ󣬶÷αˣӲʱ򣬻Щ
Сؼˡ֨֨Ҹעΰ󡣺
˳һԪԼܣǲ֪ġϵǸɣΪʶ
ϵĲʶԼίнȫȨġ
ġӢĳʲôĳλ"ѧ"ԼȨ־ѧۡ
Ŀ϶һʱ代ס˵סڳĴˣĪ֪Ī٣и
ԡûвμӹȴԳ¼֮ȫ߽񻰣
ֱһλ˼·ǳڳҲõͲűϵ˵
ɣѧңֻǸѧߡֳ񻰲
ʼ𡣵ʱһԪųڱ绤Ҫ˵ӶĿ
ɣǸѧˣɣԴġоǸҰô
ӣ˿ллô֪ӶԴ˴µ
еˡһԪ˵ѧ·һ
աʱѾȫûɱˣԱȺĸᣬǡǡα
ѧǵһձ𣿸ǵĵڽ̲αѧǵ
ǿѧͬ塣˵ĵʲôԶ

Ŀ˱ʾΪӵı﷽ʽ̫Իᱻ
ã罫ӺʹͳĻѧ¶
ܶĵˡ

˵߲ǣ߲߲壬Ӿ˵ǧ
ӡҵ⣬±⣬ֻԱ˵黳˵Լ
Ҫ˵Ļ֪Լ˵ʲôοʹ˵ʽôͬᱻ
봫ͳĻѧµȶ

˵֪Ӳں˵ĿҪĵý
Ϊ˭㲻йݺ

˵ýӹ´ȷĻҺߣźС
ӷݺӾ֣ݺ
ݺģȻȻأȡ亦飬ҲѾ
ˡ

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

ӡĽѽںҽˮĶλ

ս

ȥꡰܽؽ㡱ʱдһƪӡܽؽ
㡱С˵һ£λɵ㣬ʮˣ
ҵĿ˺һ䣺һӣѿСģ
ˡдƪµ˼ǣܽؽ㲻Ҳһͨ˰ˣŪ
Щ̬˵Щһ֮Ҳģȴƫƫҫ
˵һһǸǲɵʲôźһЩ
̬λðɵˣǸ壬˵
񵱽ּŮкһ޲ܹĶ÷Ů
˲źã͸û

쿴˷ӡһһϯ̸αѧ۵ĵڶ֣λ
˿ϾĽѽڵıݣʵ벻õıסҪٰ
ɵĵһء

Ҳ֪ѧ׵ΣͷԺδȥʱҲ
ˣ񽭺ƭӡֻôһ˵°ͺղ뱻֤ˣ
Ҳ֤ˣܽеѧˣ
䲻һǸƭӣȴǸ͵ˡһӾ뵽С˵λɵ
һһ⣬˵еĻҶﶼ
һ仰һӣĻӡ

Ȼѧ⡱ͣԶԶ˻ӡ
ͣȻó˵ҿԴ˵˵ԺܽԺ˵ǣ
ûѧרͬеϿɣûһƪڹʹϵѧȨ־ϵ
ģֻԼԼͣߣ꣩˵ʲôԼǡһ
ɵһΪô

һԽˣΪλԽҲô

ǣƫƫλСƽ￶˵Щʲôѧǲ
веġû䵱ѧĲСóʲôά˹˹˵
Щʲô߼ȵȣһӡڰðʲô뷨ԳΪ
ѧʱҲû˵ԡһٽؾ͡αѧ͡ǿѧ
˵˵ȥ˵ֻҪûƭ˵ĶͲܳΪαֻܳΪǿѧ
ܸĸαѧļһϳԼƭ˶أû
˿ϳϣ϶ĳ˾ƭƭأֻܴӿ͹۽
Ͽνоؿѧò֤򾭲
ѧ飬ȴƫƫԼǿѧô˵αѧʲô

ǸĿƵģ֪αӡǸʲô˼ָ
ȴҪװģһ·ˣɯʿǱµĴΪʲô
Ҳˡ뵱ӣֻǻûдﵽӵı׼ǡƭ
Ϊɣһ£ӸǾӡĴأԺ͡αӡ

۹⣬ѲǿѧĶΪѧαѧĳЩ
ơĳذÿѧֻ̽ĵ·ߴ˷򣬰ɵ
£ȴԼŲԼǿѧģαѧʿֻͬ飨ѽ
ڿƭɵġˮ͡ġϢ
衱Ǿʹ°ܻغģҪ׷䷨Ρ
ߴ·罯ѧͬûеõϿɣԼ
ֻǿѧģδõϵѧţСƽ
ϿѧӦһϸгԼ˵ûʸпѧ
ǷǶԴҾͬʸҲûˣҽˮȡ
֡

λνҽоĸоԱֳϴʲôѾ
񡱣ʲôɶĴ󵨻ɵȵȣȻһֱ
еĹɣȻɣѣǰҪѭѧ
Ļ򡪡ó֤˿Լ飬ظ˭
Լţ٣Ʒ˰˹̹֡һзѧȨĺ
ʽķѣô

ܽһ£

ѽڵԼӡλɵǣʵ
ɵ㣬ΪܸܿͲ죬ֻԼ졣Ϊûв
췽רҵʿ֤Ļ졣

СƽȴҪ֤˼˵˻죬Ӧǻ죻Ϊû
᲻ӵĲУûʸ

оԱҪǿǲ÷רҵʿӲ˵ӣ
ǷòõĻǲǽĴǴˡڷеġᡱ
롰ᡱĹַѾ꣡ǶַѾ

˵ʵڵģԽѽڵִ򣬾ǸҲգһ治
ȫͬ顣ϾҲϴˣ㰮õȨֵһ
ɡⶡСƽ͸λһԴξһ쵽˱
ν̣һͳҽоԺоԱҲҹĴѧνҽ
Ǹʲôˮƽ䵽ֵزˡ

ԪںԬòԽץס˶ԷϿѧҪе
ҪԬʲôųƵǿѧĸҪ㣬˷αѧҪָα
ȻѧѧĻĲв㣣ԼҪĻðѧȵȣԼ࣬
Ҫ

2006-12-30

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

αѧڷ

ˮ

֮Լǰμһһϯ̸ĽĿ¼ơСƽڱ˽Ϊ
ѧĽڣֳ⵽˺ܶ˵ɣԱѧҵ
öٵΣҪڻϵķˮƽ̫ҪǱ
Ľڣûˡܶ뵱ⶡСƽûл˵
һһϯ̸Ĳժ¼СƽĵһλԼۡ

Сƽ˵ǿѧαѧαѧʲôαѧǷ
Ϊǿѧ⡣αѧǸĸҸѧо
뾡һа취ãҸˡ˲ҪƭǮҪ
£

ǿѧαѧڴߵ̬ȡڿѧչľԣ
ѧĶǷǳġǣ˷ҪѷǿѧĶ˵
ѧɿѧǾαѧǿѧȿҲ
ʶαѧҪʲô벻⣬ʶϵĴ
ƭ

αѧΣ󵼹ڣһڵ²ϵ⡣
ΪǹҵܷҪӦáѧӦöԹб֤Ψ
αѧ˱ȻΥܷеĶԹĵҪ󣬲ǽ
辫ķǱҪԺ͵αѧ

ǣαѧǷαѧֻ˵ʶˮƽ⣬ֻ
ڼ㣬һЩǿѧݣѧȻҲ
ҪαѧģҲܾ˵αѧǷ
ֻαѧթƭǮƻ漰̷涨ķŹɷ

رӦѶСƽעǣǷ񹹳ɷһϣαѧѧû
ʲôҲ˵ÿѧթƭͬҲɷ

αѧǷԴӿշнշеĵڰ˵
÷ǳȷչӦֿѧ񣬷Ժ͵αѧκελ͸
ԿΪṫĻ֮ǿ˵Կ
յṫĻ˵ǿѧαѧ
ƭڣ𺦹档

ҴӿշڰǻӦÿԺ͵αѧĿĺȷ
Ϊ˼ֿѧ񡱡뷸ﲻûκιϵҲĳЩ
αѧƭˣԼ飬ԲŻΪαѧǷԲŻ
һᳫ½ķģڻ£󶯸
Ҫϳ

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

ҾȻһ־磡


http://www.xbaowen.cn/index.htm

ԼһǰСðڼϢңͻȻӵ˵̨һһ
ϯ̸һλŮʿĵ绰Ҳμ1228缴ٰй
αѧֳ¼ƻᡣ˵Ͻкϡ˾ϡԪ
μӣμӵȵȡҴͺᵽ⼸λ
ڷαѧϼԭͿѧ̬ȵ¸Ҿұʾ
ðתĻһȥġҲҶαѧĿҲͣ
ҵҳַ˼죬һλŮʿ绰ʵ˵
кתԲμӣ5ǰϣҲ5ʱ룬ҲΪû⡣
ҾԶشӱׯظϵʯɽų·ֳ

ķչеҵϡ˫۾⣬
ı϶ԷԵҪ˵Ҫˣݷ̨
˽ǱѧĽڣȴʱʱزأһ٣ٶش
Էķԡǣıڵʱƺ
ʹǧټƵʮ޴ػرֱ˵ĻشֵǣҲ
ĪؼԻرܡҶⳡ۵˵ġʵͼ
ʲôĻɡ

ʱܿع5㣬żҪ뿪ֳôʱڵĶԱ
δǳʱ򣬶δ˭Ҫ뿪¼ֳļαڿ˳
ظΧѸ𡣲ҵԭԼҲμӵλŮʿ
ǱʾǸ⣬ҵʱѾˣڱ뿪Ҳ˿
Ҿ͸ˡʱ˼λòⳡȦ˵ýߣҪ
ҪգȵȣҲ˴˻Ҷⳡ־֯ߵĲ
λҲμⳡŮʿ˵Ҿ˲ƽڽĿļ
ʵҽ̨顱

˴ѾһƬڣһӭ洵ʱҸеȻĿɰ
ΪĻҴһɶ

죬˸ңҵǰ˳Ȼtom.comվƼ
http://tech.tom.com/2006-12-29/04BI/64985803.htmlдΪ
һдͷңʵ˵ҽҪߡƺҵıǰ
˳ѾΪĳЩҪⳡִ׵ṩ˻ᡣЦԭ
ôһЩΨ²ҵˣһѣĿĺɡ£
һһ־أǣҪСİ

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

αѧ¼ӦеĿѧѧ߷˼һ

bluesea

Ҫ˵ĻһܴԭǿѧҹʽоԶ
ԶڶԿյĹġʵ㲻ȥھ޷˽ѧαѧ
ĿԴĻƻĻѧҵĹо

Ϻһ꣬˵ܶСľۻᣬģˮģ
ڽۣҩġҼû˵һѧҳ
սġܿսеģҲڴѧ֮ڣѧȦڡ
Ψһ˵ҲμӵҲǷͬôѧĹڻ۵Ľ
ȫĿսԵĴѧͲ֪ʶȦˡ
˭㣿

ǵĴܶǲ˽ѧҪ˽ѧʱ
򣬸λأ 

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

пƼѧѧ³Ϯ̨ѧߵ

ȶ뷢չѧۡ  ư    
人19936³棬½ԭⲻĳϮˡѧ±
֣л73ݡ

¡ȨĻȡάּƫ±еġ
ȨĺϷϷ½ȫһһδġ

Ȥϸ

һ

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

ѧһͶ

ã

һͶйѧƺʲôرˡͬѧвͬ
ѧڴڴԵĶ綨͸Ϊѡڹڷ
(Ӣİ)Ȼڹ־Ϸ(߷֮)ƺѾΪܹܵ
Ȼ߲ҹͬΪһŵоײʹԼ
ĶЩľ̫ˣ ܹڵѧܶѾ
ڹһӰ죬ڲӢİ(Ϊĵķ)ɹ
̴棬϶ܲѯõ£ڹظķ
ȻΪ ڲʱַǳֽ1Ŀ
ǰ(ȻжϺͱߵˮƽйϵ)һ5£4ƪڹ
1ƪڹ⡣ ˿Ϊʾڵѧͱһĺ󱲡
ҲϣǵĵʽˮƽԽԽá

:


Shi YH, Wang QC, Lin W

The characteristic of petrology, minerals chemistry and P-T conditions 
of eclogites from Taihu area in Dabie mountains, and its Tectonic 
significance. 

ACTA PETROLOGICA SINICA 22 (2): 414-432 FEB 2006 

Abstract: Eclogites from Taihu area in Dabie Mountains can be 
identified into HP (high pressure) eclogites, HP-UHP 
(high/high-ultrahigh pressure) eclogites and UHP (ultrahigh pressure) 
elcogites, based on the result of geological mapping (1: 10000), and 
the investigation on the petrology, minerals chemistry and P-T 
conditions of these eclogites. From HP eclogites to UHP eclogites, the 
component of grossular and pyrope in garnet and Si4+ content of 
phengites rise gradually. Peak P-T conditions of eclogites also 
transform from 535 degrees C similar to 652 degrees C, 1.50 similar to 
2.26GPa of HP eclogite, 625 degrees C similar to 777 degrees C, 2.41 
similar to 3.04GPa of HP/UHP eclogite to 767 degrees C similar to 942 
degrees C, 3.49 similar to 4.09GPa of UHP eclogites, and show a 
regional P-T gradient trend. Combine structure geometric 
characteristic in space and wall rocks of eclogites, application of 
Grt-Cpx thermometer and Grt-Cpx-Phe barometer, we define a 5 degrees 
C/km "geotherm" and two isopleth lines with T = 650 degrees C, P = 
2.50GPa; T = 750 degrees C, P = 3.00GPa, and divided the South Dabie 
Terrain into three subzones: HP-Zone, HP-UHP-Zone and UHP-Zone, which 
imply the South Dabie Terrain is a consist terrain. According P-T 
paths of three types of eclogites in this Study and previous chronology, 
we discuss different Uplift rate of these eclogites tentatively, and 
guess that these eclogites can be shortened in the depth of 40 similar 
to 50km and scaled as a "whole terrain". Subsequently, this "whole 
terrain" ascends to the crust gently and forms the present distribution. 



Shi YH, Wang QC

The peak metamorphic conditions of eclogites in the Taihu area of 
Dabie mountains and its implication for tectonics. 

ACTA PETROLOGICA SINICA 20 (3): 609-620 MAY 2004 

Abstract: The Taihu area in the Dabie Mountains had been identified as 
the conjugate area between the 'cold' and 'hot' eclogites, we have 
carried on geological mapping in the Tailm area of the Dabie Mountains, 
and investigated on petrography characterists, variance of mineral 
composition, K-D-value and the peak metamorphic P-T conditions of the 
eclogites in detail. This study has shown that the eclogites in Taihu 
area can be divided into three types from south to north: 1 
Zhujiachong-type eclogite; 2 Daba-type eclogtie; 3 Jinheqiao-type 
eclogite. An obvious gap of the peak metamorphic P-T conditions 
appears between the Zhujiachong and Jinheqiao-types, with the average 
values of P-T conditions of the Zhujiachong-type eclogite being P = 
2.14GPa and T = 563degreesC, and that of the Jinheqiao-type eclogite 
being P = 3.76GPa and T = 791degreesC. The Daba-type eclogties are 
distributed around quartz/coesite phase transition in P-T conditions, 
which, tectonically, is equal to high-ultrahigh pressure transition 
belt. The Zhujiachong and Daba-type eclogties correspond to the 'cold' 
and 'hot' eclogites separately. They show a good continuity in the 
respect of the peak metamorphic conditions and no obvious pressure gap. 
Hence, we consider that the boundary line of the 'cold' and 'hot' 
eclogites does not exist. 


Shi Yonghong Wang Qingchen

Peak metamorphic conditions of the high2ultrahigh pressure terrain in 
south Dabie mountains

CHINESE JOURNAL OF GEOLOGY 2004 39 (3) :375 -387

Abstract: For a long time , many geologists accepted the opinion that 
the high2ultrahigh pressure metamorphic terrain in the south Dabie 
Mountains was composed of thecoldandhoteclogites ; however 
,some different arguments still exited about the relationship between 
the both. This study tried to reveal the geological architecture of 
the high-ultrahigh pressure metamorphic terrain in the area of south 
Dabie Mountains in the light of peak metamorphic P-T conditions of the 
eclogites. The studied area was located at the Hualiangting reservoirs , 
Taihu County , where outcropped four types of rocks from the south to 
the north : the mica2schists , the biotite gneisses , the granitic 
gneisses and the epidote biotite plagioclase gneisses. The eclogites 
occurred as lens , blocks and/ or layers in the later 



SHI Yong-hongWANG Qing-chen LIN Wei

The peak P-T conditions of eclogites from Taihu area in southern Dabie 
and its tectonic implications

Acta Petrologica Et Mineralogica 2006, 25, 127-136

On the basis of petrology,mineral composition and peak p-T conditions 
of the eclogites from Taihu area in southern Dabie terrain,the authors 
hold that southern Dabie Terrain is composed of three metamorphic 
zones,namely,the ultrahigh pressure zone,the high/ultrahigh pressure
mixedzone,and the high pressure zone,with a regional p-T gradient 
trend.Five Grt-Cpx thermometers and Grt-Cpx-Phe barometers were used 
to evaluate the peak p-T conditions of these eclogites. Four p-T 
regions have been identified,and their  


Y. SHI and Q. WANG

Variation in peak P?T conditions across the upper contact of the UHP 
terrane, Dabieshan, China: gradational or abrupt?

Journal of Metamorphic Geology 24 (9), 803-822.doi: 
10.1111/j.1525-1314.2006.00670

Abstract:The Southern Dabieshan Terrane (SDT) has previously been 
divided into high-pressure (HP) and ultrahigh-pressure (UHP) terranes, 
and its regional extent and the tectonic nature of its boundaries are 
hotly debated topics. In this study, an eclogite-bearing area of 100 
km2 near Taihu is mapped in detail, and divided into Northern, Middle 
and Southern Zones on the basis of lithological characteristics. The 
Northern Zone consists of epidote-biotite gneiss and eclogite blocks, 
the Middle Zone includes granitic gneiss, biotite gneiss, eclogites 
and amphibolite, and the Southern Zone is composed mainly of 
garnet-bearing 

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

ߡ

jian

˿йءߡתαʿµҲԼ
־һЩϴѧǰϲ־ǡժڶ
ռ档ΪԭⱾ־˵־
¿ֳʲôũҲˡ

ҵһ˵ɵˮ񻰾ǿⱾ־תйʦ¼
ĳƪ¡ʱһǴѧѧרҵ꼶ѧΪԼѧ֪ʶ
ôҲ벻ͨˮôܹ׵ر˸ȼϣðظ־༭д
˷µʵԡȻûյκλֻΪ༭Ͼ
Ƴⶫ˽⡣ߡֿһƪ£
һεʱλ̤ԱΥҪ
ȻȫСԱһµİ
11ϵİķ˹ʵȫͬظ༭ȥ˷ɴ£
Ȼûл֪ʶһƪרŽ¶³ƴֻһ
ƪƻС˵ڲٱʵʷأýĲϽ
ߡȻûзйشֻС˵༭Ҳǰ
ˡԺҽԶˡߡΪı༭ȱĿ
ѧͶʷĿ͹̬ȣҲΪⱾ־Сʻ׷
ĵɿ顣żһη˱µġߡַһƪЦ
¡1967424ճ1ŷɴصʱɡ϶
Ա޷Ĺ̴۸ĵһͿ˵ʲô޷緢˽ɡ
ϣʱսѺͼ˱׳ظָ
Ǹȡ½ĳЦΪ׼ҲͲΪ
ˡ

ˮƭ˲ٿѧҺԱС༭һûʲôС֡
дĵС˵ıʲҲ©١ƼʷӦһۿ
ʷʵ˵֤²Ǧһһڼѡڿ
Ĺһ׾ӵĻԺͶʷ󵼶ߣҼ
Ϊ̫ҵӢۡԾЩΪߡı༭ڻ
ѧϲˮƽܵͣԽԽͣ˵ǡǡֻͬˡ

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

Ϊд̤߼

컢ЦХ
2006/12/30

޼2006/12/30ڡ˿ϵ£еɡİ
ʵԡĺڡźģ¶䣬ָ
Ϊд̤߼ΪʵʵھߵԷҲû
ָĸλѧңǲеҵƭӵɣ

ȰƵļߣҪΪдϹ죬뵽ʵȥ
ע²ϰյļ࣬ȻܹдиȾĺ¡עһڵ
ʮúĿ󹤣עһºյУ¼ȡ֪ͨ飬
ѧѶɱļҳ

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

ҩ˵

á

ҽڲý忴ҽıۣһ϶Χҽ
ۺֿ֤ۡ˵Ҫһ֤ҩЧԡҶҽѧ
˽⣬ҽѧѧԡҵĿãʹҽǿѧģĿ
ǰҩļҲҽβ

˾סϷһСУǹһҪӹ
ҩĵĻأǰCCTVԡѬעˮҩġعȻ
ΣɣǱص֧ҵԵطǷ
ġÿܵĶҲ޿κΡЩҪβ
ҩģݺѬȻ¶ĳɹЩؾ
̳·ϡԱߣ泣мèСɹĹ
Ҳý淭ҩġﾭͻ±꣬˵ˮˮ
ҩѹܵˣҩȾǳе顣룬ʹͨʳƷ
ӹ嶼кģοҩƷأ

ط֪ҩӹ˶ȥҩʹԭҽ
һˡһЩͬѧҩģǽȫ
󣬶ѬҩѾǱؾĹˡиСһβμͬѧ
ϯһƷ˷׷ƷΨһλҩĵͬѧ
ԭ֪ϴǾǡƯסġ㿴ҩ
ǹʱҲȥԼҩɡ

粻ţGoogleһ¡ҩ ǡҲԼ

ף2007֡

һxys

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

ҵܺ

Źҫ

áٶҵΪؼһ硣ҷ֣
ϿɱҳѾ7ʹҸеǳȡ
ص˼һ£һԣһλҽɡ
ʿ˵ҵˡꡱˡԴˣҷǳҪ岻ɡ

ҹƣҷһûмҡңһ
˵˵ʵҵܺãûκΡꡱļ

ȥ꣬ұ״μָ֬ƫֵ2.5Ѫѹʱﵽ
140/110ûеڹ130/90ġΪأѾˡٽġ
Ĳ״̬꣬ұƵˡҽ֮ķ˼ϡΪˣҵѧ
ͬ¡ͬжΪҵ嵣ġҵһЩͬºҵѧҽԺ
ҽƼһЩƷֻзð˹ƥֽ
ѪСһƴʩ񡰵Ƭε衱֮гҩ
5ԪǮһġѹҩҴǲмһ˵ġ

ʵϣԴұಡ͸ѪѹԺҾԼоνе
ˡĶ˰ؽ˹ҽдġ˥ʳһ顣ΪȷⱾ
ɿԣеĲοǷʵҳ飬
оݿɲġˣΪⱾĿɿġҰհؽ˹
ҽĽܣͨһЩǴҩԼ״̬
ûгһƬѹ顱֬顱顱֮ࡰͨ󡱵ġ顱
ҩ11·ȫУְʱҵಡ͸Ѫѹ֢״ȫʧˡԭ
140/110ĸѪѹڽ110/80ԭָ֬ƫֵ2.5
ߴ7.8ڽ0.9(ֵΪ0.52.5)ĵͼ֣Ҳʾҵ
ĺã30˻Ҫá죬ʹҼᶨţһ
ûеꡱĵز

ŷҡ֪ǾԷġҲΪһֱе
֪Ҳѡ׷֪ʶΪҵְҵλŷˣΪѾ
˳ֵ֪ʶˣԾòÿ춼׷֪ʶ׷
е֪ʶҪе֪ʶͷƷ㣬׷ɿˡ˼˵Щ
֪ʶӡ룬ǳͳڲԡ֪ʶΪ㡣ԣ˼
֪ҡȫġЩҽɡ
ҡꡱǾԲġȻǿԱһԽҰܣ
һɽгҲС

ϣһҵ״ˣһ
ҵľ飬Ҫһ㣬ѧؿѧһЩ
ж֪ʶĿɿԵķԱäĿȥЩȥûʵȱ
ȷԵġ֪ʶԾαѧţҪЩ
ƭӣҪʹЩ׵ġợΪΣ
ȫġ첡̡

Ҫˣϣλµһעȫ彡

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

ġɫ֤Ĵ

ߣĽ

ܶʦ֤ʱץס""ĶԼ""
Ȼڶ"""ȫ"ʱңģ"ƽ
5"ΪɵXΪⲢĴ
пܱġ"ȫ"ͨʽȼ۵Ķ壬Ǹ"
1"ʵһ֤ѡʦܴ"ƽϲ
5"ü򵥵ķ֤ɫͬѧ
Ĵ¡ 

ʦƪ³ǰҾԤԣʦ󣬲Ҳ
ֲĴ󣬻"ƽϲ5"ƵɫĹС
ٴϺܶΪĹһԵȼɫע⣬
Ƶ̵Ѷȿ˵൱ɫ

һ䣬ʦ֮ǰġǡУƻ棨̥
棩5ڣʵϺ׻7ڣ
ɫһƽɫ򵥵ö⣬100ǰѱ֤
˱ɫɫ)ڻи˻7
ڵĹͼȻһʧˣ֪ǲǱʦɾˡ

ʦڸ˴""Ƶɫ"֤"
ͼ"ɫ"ĹʽƵȻԤһʦﷸ˲
ֲ

ʦָ
"DʾڣżȫΧͼ
ʾ"
"еDDBϵͳҲͬԲ֤
"
"壺ֻɫɷֱĵͼϵͳɫԵĵͼ
ϵͳʾΪBϵͳ"

ôʦ˼˵"ڣż
ȫΧϵͳֻɫɫ""ڣż
ȫΧϵͳ"仰Ƚֿڣʦ׿ͼʾ
"ϵͳ"ָһͼмһΧΧ2nnȻ
2n>2)

էһһ"ϵͳ"ȷʵֻ3ɫɫֻҪм䱻Χ
һɫΧż2ɫɫͿˡȻ
ʦһĪļ裬ǼΧмЩ򣬳
""мӰ⣬ɫȫܵӰ졣
ʵϣһӵĵͼϵͳУּ貢ô"Գ"ġһ
򵥵ķһ4ΧΪ㣬Ϊ4
мңôʦ"""Bϵͳ"
3ɫɫ4е
ǲġȻǷ֣£ɫ޷Ⱦɫġ 

ļ"DͼϵͳCϵͳ""Dͼ
ϵͳͬCϵͳ"ҲͬĪؼٶΧмЩ
ɫʱܵ"м""Ա"ӰĴʵϣɫɫ
ͨ"ϵͳ"򣬿Լ临ӵķʽɫƣû
ɼ򵥵϶ȥûֱڵɫǶġﲻ
ü򵥵ķֱ۵طˣΪʵ"ɫ"ȷģԾٲ
5ɫȾɫķ 

ϵģʦ⼸Ҫ˵ƺǣ"ÿϵͳɫ
ʱǲȲҪϵͳΧԴϵͳɫӰ"Ȼ
ʦóÿ"ϵͳ"һͰΧɣ
ɫɫ

˷ָ鷢ˣʦƣ"Ϊһеͼ
ֽΪɫԡɫԺɫֵͼϵͳ֮ͣԵͼɫ
ȫΪɫ"

ѵͼֳСͼÿһСͼУÿСͼе
򶼿ò4ɫɫǷζŰЩСͼһҲò
4ɫɫҲ˵һͼСͼÿСͼ
һ4ɫɫôǷζŰЩɫƴ͵õͼ4ɫ
ɫ

ûô򵥣ΪЩСͼ֮Ҳб߽磬"ֲɫ"
ƴͼʱпܻСͼ֮б߽ɫͬӶ
ʹɫҪ

ֿһʦġйͼоһģʦڰѵͼ
ϵͳСͼʱһڶСͼеģȻͼÿ
Сͼ4ɫɫɫڵǣÿڸСͼ
ɫУӦһɫܹ˵һڸСͼɫУʹõ
ɫͬģ֤ͬôЩСͼɫƴ
ͼɫ

֮ܶСͼ4ɫɫƵͼ4ɫɫô
1  Сͼ֮ظ֤ƴɴͼʱСͼ֮ı߽
򲻻ͬɫ
2  Сͼ֮ظ֤ԳڼСͼеһ
Сͼɫܹͬһɫ

ܼ򵥵ش"ֲɫɫ"ʦ֤Ҿ̫ˣ
ֱӰѵͼ÷飬ÿΪһСͼÿСͼֻһ
ɫɫƴǾ͵õ"һɫ"

ЩΪʦ"һոµļѧǰû뵽
˼·֤ɫ˼·ܻѧķչҪӰ"
˵Ҫѧǵˣˣ

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

ӹɫ֤ɫĻ

Yush

ɫƽϵĵͼơһάռ䣬ֻöɫ
߶ΡڸϣƵͼҪɫɫ
http://en.wikipedia.org/wiki/Four_color_theorem#Generalizations
⣬ɫƹ㵽άռ䣨磬ÿɫƤͬʱ
Ƥӣ

νڼѧǡеȫֵΪ4
ƵƽϵɫôҲ«䡰
еƳһάιά͹ġXɫ

1. ߶ȫֵΪ3ܹƳһάġɫʵ
ֻҪɫ
2. ݻιȫֵΪ5ܹƳιϵġ塱ɫ
ʵڻιϻͼҪɫ
3. ݡ͹͹ȫֵΪ6ܹƳ
ά͹ġɫʵϲάռġXɫ

ˣҪôνǡ˽Ҫô䡰
ƵɫĹǻġ


1. ֺͷġڼѧСǡ
㣨ֳ̫ȫ 1
żӣֳӣȫ 1 2
߶Σֳңȫ 1 2 3
ƽ桢棩ȫ 1 2 3 4
ι棩ȫ 1 2 3 4 5
͹ȫ 1 2 3 4 5 6
ȫ 1 2 3 4 5 6 7
ȫ 1 2 3 4 5 6 7 8

2. ƽ⡰ɫ롱֮һ
ƽϵĵͼҡʡȣ
ҡʡȣ಻ͬȫڵĹϵ֮Уȫ
ֱڣȫڵĹϵ֮С
ʵǰڼѧСǡеĵ
ָʾݡ

Դhttp://liming1944.blog.sohu.com/

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

ǿҽָ崫ͳ

ƽ®

ǰ꣬ͨ͵׾ַɹԡ֮ȡ崫
ͳաڡŴųɹһʱٹͬ飬
꣬־֮ʿָӦһǵһǣĻŲ
кͷ﹤һЩͬ־Ǵָҹ
Ļͳһ̵õ˹ѵӦ֧֣

˶ҹǧ崫ͳƻԹСţ
˷˶ٳ߰ײѽᳫ׻ģ˶īֽѽϳƾƣû
ĲӰǷ԰ֻ˶޹Ů԰³Ѹ
ˣĭˣʯҲˡô˰
ŮȨ߲޷ŭĴ:У 

˽ޣ֮ңһʰ 
ըƽ®ɽֹͣת֮ơɱйֻ֪֮һʱ֣
ư֮һꣻֻ֮ﾺ񣬶֮ƽ
 

ᣬ£ɥӣѾ𡣻ָ
 žڱС֪̲ǵһ֢
δˣΨһİ취ֻԤָֹ
Ϊһð취ָ̣Ů潣вΣֹ
ẓ̵̌ԲȻ޷ԲȻɳ 

̳Ů࣬˵һ֤Ҳڻ
㣬Ե޷ߣȻǻָýǣߣĸ֮
£ɸ㶨ΪŮӣò޵£ĸϣγ޿
ӣ޷޳ý࣬λһޡ 

ƴ޶ƯһΪūεӰֻƣ 
жŮӣܲȻƶϣ˽Ų
ġ䲻ҹ˳ҵƻ𣬵˭иůļأ
ƶȣҵȻòٴ 

޵ܡ˼ߡ˼ʲôѽ 

޵ش˵˼ôãΪʲôйҪϳأ 

־Ħ½СˣֲֻԸ˷۱
ʹ̷˼ŭĳٱš 

ģˣ 
 
Ļ֣ 
! 

ָ˳Ӧģ 
崫ͳ岻ݴǣ

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

˼ҹ

x8b8x8

ѧõģѧвдһʱİáһʱ䣬ĳЩѧ
۳ŪʲôָָΪѧ½չҵ˿֪
һգʱͻȻ£룬˵ڻʱӾһ
רңҺβҲһ£û׼Ҳܳɸָרʲôġ˭֪һѣ
ȴѳһӲʱˡ

ԭԻʮĩʮͳһλʿѧ
˼˵ԷֹɣһǸΪŵָһ
ΪŵָָָĹϵǲ֤ġ˵ȥ
ͦµģĥĥȥʵ˵ֻԵĹϵ͹
ˣΪ˶ġ͡塱ָָ
ˣתһ룬Ҳרѧǵͨлú˵˵ˣ
ʲôҪһ˵ϰϾͶרѧ߾ûˡԼѧרҵ
ƺҲòᣬҲȻˡ

ⱾԼüҷһۣ֪ͨѧϲŪ顢
ݵķԽҲֹɧһҲͰˡû룬ҹ
һΡ

ϡǵһĴ⻷൱ģȴһ˵
˼䣬θʣһǧذתѰ϶ͻΧǼæһƧ
ųһƨܼ䣬Ȼһ߶
⶯״Ҵ󾽣æԼ֪ڴˣղ
Ϊʵǹ⡣Ҳȣ˰֣ȻŵصƬ
ֻƬȻӡšƨ⹹ʦͷΡ߽
ͷξδţֻС̣Ǵʦ֪кμ̣

    ͵ܸղ֮ƨϸϸ⹹볣˴ͬһȻþ
Ҳδɴƨ˵ƨ¹ŵ̼ɡִ
ɡ

    һ֪һαѧʿˣǴ˵⣬ƨ
زͬԭ֡£ˡܷ㡣

    ȴһס˵ԴƬ̣˵꣺ƨȻأȴ
Сӳ˵ƨɷ硯ϵУųͳƨߣĳ
ˣĳĳ꣬ĳĳ꣬ĳĳĳĳ֮󣬴˳ͽεɷ
չͣÿַΪ߸֧͡ϸ˵ƨڵڶ͵
һ֧ͣѧСɷ磭21Ŀǰܷųƨ˲࣬
ĳĳĳĳĳĳĳĳĳĳĳĳлǰȥ̽ãػᷢ
ЩζͶ

    ˼̸²ףͶ㶼͸ѧʣʲôãҪӪ


˵꣬Ͻм䣬̧ȣˡ

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

ͥ羻ҽѧ ٷ
С״桰Ҽߡͥ 
ҽѧרҵ÷ٺͼֱѶ 

20061228աɶ

һǽڣһоԱҼȲǽڣҲоԱ
10ʱС״绪ŷȨһ
ԺͥĴͥһǣԭ
ѧߵݣʹϵȨۣһѧרҵۡԭ
ʱԳݡۣͥϵķ١ԱԼļߵȣһֱ
Ρ 

ϵ֮ 

ҼµĹϵʲô 

9ʱͥʼԭС켰ʦͱ绪
ʦͥμϡһŷݡû¶棬ίдʦͥ 

Ϊԭ棬С켰ʦȡѡΪȥ1231գ
绪ŷݵ6׫дͨ˿վһƪĿΪĴѧ
С<Ȼ>־ˣλƭҪNature Biotechnology(<Ȼ>
־)ͬ͹ͬȨ£ȫʧʵС˸
裬ѹ˶СȨֺСΪš
ŷ˸вжΡ 

Դˣ漰ʦΪšŷ˵ȷǩȻдţ
С2003ǵ6˹ͬڡȻϵѧ顣
ʾ˿վƪҼ£Ǻ֪顣Ϊˣ淽
һ̩˹˾˵飬֤ʵ̩˹˾ֹ˾Źڣ
šŷûκιϵ 

֮ 

ѧǷм٣ 

С˵417գĴѧרСʵý
СС١Ϊ֮6º12£Сȥ
롶Ȼ־־ϿĴѧʵϵĵ
ʵԡСʾķκʵĿѧȫ֤
оɹĿѧԺʵԲκɡ 

Դˣ淽ΪСֱӵϵʵ
ӦΪ֤ݡͬʱʾС쵱ڡȻ־ϵġ
۵ϣûʵҩЧѧʵݡ淽
ʾҪʾȥ2ػҩҵŹ˾
PH-SAҩѧооۣڵ6Ҫ
ΪƾԡԵľмǿԵPH-SA
١󣬱淽ҪСоɹ˾ 

֮ 

6˷Ϊֻ2ˣ 

ڷͥϣС켰ʦΪνҼ֮㡢Ӱ
Ƿ߱˾ǡ١绪ŷݵ6ˡС
˱ʾΪⳡѧٷ粨ýΪй
ĿǰѧߣѧĹ㷺ע
ͬʱҲӰСĹڴˣС򱻸޶
ľ⳥5Ԫ 

Դˣ淽Ϊд鲢ǽΪ绪ŷݶΪ
̩˹˾¡4Ա淽Ϊµ4
Լ̩˹˾ҲӦ׷Ϊ档ԭΪ˷ѡ˭Ϊ棬ԭ
Ȩ 

֮ 

Ա֪μͥ¼ 

ΧǷ٣С绪ͥչ˼ұۡͥϣ֮
ġԡPH-SAҩЧѧרҵʻ㡢ҩѧ۲ӿⳡ
ȻѾһȨǷıۣͥ󼸺Ϊһüѧ
ۿΡԴˣгҡͷ˵òרҵۣҪ
ع鵽ķɱͥУ漰ѧ̫רҵר
ʻɬѶԱòгָ£¼ͥݡҲ
Ƕǡ 

12ʱ20֣гͥ

(XYS20061231)

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)

һΪ˰޷˿վĹ˽˿վĶ̬ؿ
˿ʼбxys@yahoogroups.com

ʼбÿ췢һ˿վ¸µϣÿµ׷һÿ
Ŀ¼ʼбĶμ롰˿֮ѡ
ʼбxys_friends@yahoogroups.com

ù䶩ġù䣬ܿ޷յ
Ƽ䣺yahoo.com, hotmail.com, gmail.com

ġ˿ʼбĵ䷢һհż

xys-subscribe@yahoogroups.com 

塢ͣ˿ʼбͣ䷢һհż

xys-unsubscribe@yahoogroups.com 

Ͷxinyusi@yahoo.comôıļͶ塣

˿(www.xys.org)(xys.dxiong.com)(xys.3322.org)(xys.xlogit.com)